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spectral decay parameter

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Journal Article
Published: 25 October 2022
Bulletin of the Seismological Society of America (2022) 112 (6): 3037–3045.
...Raúl R. Castro; Daniele Spallarossa; Francesca Pacor; Leonardo Colavitti; Giovanni Lanzano; Claudia A. Vidales‐Basurto; Sara Sgobba ABSTRACT We investigated the temporal variation of the spectral decay parameter κ before and after two main earthquakes that occurred in the central Italy region...
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Journal Article
Published: 27 April 2022
Seismological Research Letters (2022) 93 (4): 2299–2310.
...Raúl R. Castro; Leonardo Colavitti; Claudia A. Vidales‐Basurto; Francesca Pacor; Sara Sgobba; Giovanni Lanzano Abstract We study the spectral decay parameter κ using S ‐wave recordings from the central Italy dense regional array. The data set used consists of 266 earthquakes, 353 stations...
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Journal Article
Published: 01 February 2010
Bulletin of the Seismological Society of America (2010) 100 (1): 196–206.
...Avelina I. Fernández; Raúl R. Castro; Carlos I. Huerta Abstract We calculated the spectral decay parameter ( κ ) in the southern Basin and Range province, using records from earthquakes located near the Pitáycachi fault. We found that for a given distance and recording site the values of κ vary...
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Journal Article
Published: 01 December 1991
Bulletin of the Seismological Society of America (1991) 81 (6): 2186–2193.
...John G. Anderson Abstract The spectral decay parameter, κ, defined by Anderson and Hough (1984) is described as a function of distance, R , and site, S , as κ( R , S ) = κ 0 ( S ) + κ˜(R). The terms κ˜(R) and κ 0 ( S ) are found by a method that is unbiased by prior assumptions about the nature...
Image
An example of the spectral decay parameter in the natural logarithm of normalized amplitude acceleration Fourier amplitude spectra (FAS). (a) Individual normalized acceleration FAS (gray lines) and its average (solid black line). The horizontal‐to‐vertical spectral ratio (HVSR; red dashed line) and a line indicating no site amplification (HVSR = 1; black dotted line) are overlaid. The resonance frequency and its HVSR value are listed in the legend. For each station, frequency limits were manually established to encompass dominant linear attenuation (fm1 and fm2; blue dotted lines). (b) A result of κ estimation for an event. Raw and smoothed spectra are shown as gray and black solid lines, respectively. The initial corner frequency (fc; cyan dotted line) and frequencies of the start and end of the linear slope (fE and fx; gray dotted lines) are shown. The regression result (red dashed line) between fE and fx is plotted. A figure title indicates event ID (including magnitude), network code, station code, and data component. The color version of this figure is available only in the electronic edition.
Published: 11 February 2025
Figure 2. An example of the spectral decay parameter in the natural logarithm of normalized amplitude acceleration Fourier amplitude spectra (FAS). (a) Individual normalized acceleration FAS (gray lines) and its average (solid black line). The horizontal‐to‐vertical spectral ratio (HVSR; red
Image
High‐frequency spectral decay parameter kappa (κ) measured from the vertical component of the acceleration spectra of regional event R1. (a) P arrival for κp,acc and (b) S arrival for κs,acc. The spectra are stacked among stations within a subarray of a 2.5 km diameter circle (15–20 stations). The signal spectra (colored) are calculated in a 1.5 s window around the P or S arrivals. The noise spectra (black dotted) are calculated in a 1.5 s window 8 s before the P arrivals. The thin colored lines are linear fits between amplitude (A) and frequency (f) for estimating kappa. We require a minimum frequency bandwidth of 15 Hz. See Figure 2 for the criteria for determining the frequency range. Only one‐fourth of the total spectra and fitting are shown (equally spaced across the array) for visualization. The color version of this figure is available only in the electronic edition.
Published: 03 January 2025
Figure 3. High‐frequency spectral decay parameter kappa ( κ ) measured from the vertical component of the acceleration spectra of regional event R1. (a)  P arrival for κ p , acc and (b)  S arrival for κ s , a c c . The spectra are stacked among stations within
Image
High‐frequency spectral decay parameter kappa (vertical component): (a) κp,acc and (b) κs,acc, and (c) their comparisons. The kappa values are the median of regional events R1–R3. In panels (a) and (b), each colored circle represents a subarray consisting of stations within a 2.5 km diameter circle (15–20 stations; small, black, hollow circles). The color ranges exclude the 1% lowest and highest values for visualization. The contours indicate the boundaries of the surficial Quaternary formations (Q) versus the Permian formations (P). The error bars in panel (c) are the standard deviation of the fitting. The spectral decay is mostly site‐dependent, with the Quaternary sediments being more attenuating than the Permian rocks. The color version of this figure is available only in the electronic edition.
Published: 03 January 2025
Figure 4. High‐frequency spectral decay parameter kappa (vertical component): (a)  κ p , acc and (b)  κ s , acc , and (c) their comparisons. The kappa values are the median of regional events R1–R3. In panels (a) and (b), each colored circle represents a subarray consisting
Image
Dependence of spectral decay parameter on epicentral distance (R) for longitudinal and transverse components. The color version of this figure is available only in the electronic edition.
Published: 01 February 2013
Figure 6. Dependence of spectral decay parameter on epicentral distance ( R ) for longitudinal and transverse components. The color version of this figure is available only in the electronic edition.
Image
Distribution of spectral decay parameters with focal depth for the selected stations, showing the depth dependence of spectral decay parameters at shallow focal depths. The mean and one standard deviation of each distance bin are plotted as squares and vertical lines, respectively. The regression line within 3 km is represented by a red dashed line. The color version of this figure is available only in the electronic edition.
Published: 11 February 2025
Figure 13. Distribution of spectral decay parameters with focal depth for the selected stations, showing the depth dependence of spectral decay parameters at shallow focal depths. The mean and one standard deviation of each distance bin are plotted as squares and vertical lines, respectively
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Distribution of spectral decay parameters (black dots) as a function of (a) epicentral distance, (c) magnitude, and (e) depth. The mean and one standard deviation within each distance bin are plotted as squares and vertical lines, respectively. (b, d, and f) Heatmaps corresponding to panels (a), (c), and (e). The color version of this figure is available only in the electronic edition.
Published: 11 February 2025
Figure 3. Distribution of spectral decay parameters (black dots) as a function of (a) epicentral distance, (c) magnitude, and (e) depth. The mean and one standard deviation within each distance bin are plotted as squares and vertical lines, respectively. (b, d, and f) Heatmaps corresponding
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The relationships between κ‐values, magnitudes, and variables related to frequency windows. The red dashed lines in each figure represent the regression lines corresponding to variables in each figure with the Pearson correlation coefficient (r). (a) Spectral decay parameter values versus magnitudes. A red dashed line represents the regression line. (b) Lengths of frequency windows versus magnitudes. (c) Center frequencies of windows versus magnitudes. (d) Spectral decay parameters versus lengths of frequency windows. (e) Spectral decay parameters versus center frequencies of windows. (f) Center frequencies versus epicentral distances. The color version of this figure is available only in the electronic edition.
Published: 11 February 2025
Figure 10. The relationships between κ ‐values, magnitudes, and variables related to frequency windows. The red dashed lines in each figure represent the regression lines corresponding to variables in each figure with the Pearson correlation coefficient ( r ). (a) Spectral decay parameter
Journal Article
Published: 10 March 2020
Bulletin of the Seismological Society of America (2020) 110 (2): 452–470.
... model (commonly used in worldwide), the exponential spectral decay model, described by the parameter κ and the specific frequency f E at which a spectrum starts to decrease linearly with increasing frequency in log–linear space. For large earthquakes, we estimated f max to range from 6.5 to 9.9 Hz and s...
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Journal Article
Published: 03 January 2025
Bulletin of the Seismological Society of America (2025)
...Figure 3. High‐frequency spectral decay parameter kappa ( κ ) measured from the vertical component of the acceleration spectra of regional event R1. (a)  P arrival for κ p , acc and (b)  S arrival for κ s , a c c . The spectra are stacked among stations within...
FIGURES | View All (13)
Journal Article
Published: 01 August 2012
Bulletin of the Seismological Society of America (2012) 102 (4): 1796–1809.
... contradictory results and suggest that there are still unresolved aspect on the origin of high‐frequency spectral decay. Investigations into the attenuation parameter κ of local earthquakes in southeastern Sicily were performed by Tusa and Gresta (2008) . The authors computed the parameter κ from...
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Journal Article
Published: 17 December 2019
Bulletin of the Seismological Society of America (2020) 110 (1): 295–311.
...Seon Jeong Park; Jung Mo Lee; Chang‐Eob Baag ABSTRACT The high‐frequency spectral decay parameter kappa ( κ ) is estimated for the Gyeongju area using records of the temporary seismic array in the Gyeongju area (TSAG), which operated from 2010 to 2013. Gyeongju is a city located in the southeastern...
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Journal Article
Published: 01 July 1991
Seismological Research Letters (1991) 62 (3-4): 201–209.
... parameters can be resolved for events with moment magnitudes in the range M W = 3 - M W = 6. For smaller events (M W = 1 - M W = 2), moment and spectral decay parameter are still well determined from low frequencies in the data. The average corner frequency is stil reasonable in this case...
Journal Article
Published: 24 May 2016
Bulletin of the Seismological Society of America (2016) 106 (3): 1342–1356.
... of this figure is available only in the electronic edition. 20 March 2016 The attenuation of ground‐motion acceleration at high frequencies is often parameterized by the spectraldecay parameter kappa ( κ ). Kappa was first introduced by Anderson and Hough (1984) to model the high...
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Journal Article
Published: 01 August 1992
Bulletin of the Seismological Society of America (1992) 82 (4): 1622–1645.
... source and an exponential decay term, e −πκ f , to describe the high-frequency spectral shape. The spectral decay variable, κ, associated with attenuation, is parameterized as the sum of a distance dependent component, κ ˜ ( r ) , and a site term, κ 0 ( S ), which takes a different value for each site, S...
Journal Article
Published: 01 February 2013
Bulletin of the Seismological Society of America (2013) 103 (1): 223–235.
...Figure 6. Dependence of spectral decay parameter on epicentral distance ( R ) for longitudinal and transverse components. The color version of this figure is available only in the electronic edition. ...
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Journal Article
Published: 01 February 1997
Bulletin of the Seismological Society of America (1997) 87 (1): 97–113.
... of subfaults, each of which is represented by a Brune omegasquared point source, correctly matches the observed spectral shapes and amplitudes. The spectral decay parameter kappa, representing average near-surface attenuation of high-frequency motion at rock sites, increases with increasing magnitude, from...